Response to the comment by M. Lustrino on “High-pressure melting experiments on garnet clinopyroxenite and the alkalic tholeiitic transition in ocean-island basalts” by Keshav et al. [Earth Planet. Sci. Lett. 223, 365 379 (2004)]

Details Response to the comment by M. Lustrino on “High-pressure melting experiments on garnet clinopyroxenite and the alkalic tholeiitic transition in ocean-island basalts” by Keshav et al. [Earth Planet. Sci. Lett. 223, 365 379 (2004)] Response to the comment by M. Lustrino on “High-pressure melting experiments on garnet clinopyroxenite and the alkalic tholeiitic transition in ocean-island basalts” by Keshav et al. [Earth Planet. Sci. Lett. 223, 365 379 (2004)]

Jan 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006e%26psl.241..997k&link_type=abstract

Earth and Planetary Science Letters, Volume 241, Issue 3-4, p. 997-999.

Physics

Scientific paper

We welcome the comments made by Lustrino [M. Lustrino, Pyroxenites everywhere, Earth Planet. Sci. Lett., this issue.] on the high-pressure experimental melting phase relations of anhydrous garnet pyroxenite reported by Keshav et al. [S. Keshav, G.H. Gudfinnsson, G. Sen, Y. Fei, High-pressure melting experiments on garnet clinopyroxenite and the alkalic-to-tholeiitic transition in ocean-island basalts, Earth Planet. Sci. Lett. 223 (2004) 365 379.]. Such healthy debates, in our view, are needed to promote our understanding on the origin of oceanic-island basalts (OIB).

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